山地学报
山地學報
산지학보
JOURNAL OF MOUNTAIN SCIENCE
2015年
4期
441-448
,共8页
王磊%邓青春%张斌%刘辉%刘刚才%罗明良%舒成强
王磊%鄧青春%張斌%劉輝%劉剛纔%囉明良%舒成彊
왕뢰%산청춘%장빈%류휘%류강재%라명량%서성강
竖井%形态%演化过程%控制因素%干热河谷
豎井%形態%縯化過程%控製因素%榦熱河穀
수정%형태%연화과정%공제인소%간열하곡
vertical hole%morphology%evolution%controlling factors%Yuanmou Dry-hot Valley
竖井是一种特殊的潜蚀地貌类型,是大规模土壤侵蚀背景下不容忽视的灾害性环境问题。竖井的发育是冲沟侧蚀后退的一种方式,对冲沟沿线形态影响巨大,研究其成因和演化过程对认识冲沟的侧蚀和后退机制具有很大的参考价值。基于对元谋干热河谷沙地村竖井群的实地考察和测量,将竖井的发育划分为萌芽期、扩张期、完整期、破碎期和残夷期5个阶段,不同发育阶段其平面形态与剖面形态具有显著的差异;完整期竖井的形态最具代表性,其长度、宽度和深度的变化范围分别在0.75~3.29 m、1.01~2.84 m、1.98~10.26 m,长宽比在0.3~3.1;竖井的形态与发育过程主要受到降水和地表径流、构造、土体性质、地形与植被等因素的控制。这一研究有助于认识竖井的形成与演化,也为实践中工程地质灾害防治与沟蚀监测提供科学指导。
豎井是一種特殊的潛蝕地貌類型,是大規模土壤侵蝕揹景下不容忽視的災害性環境問題。豎井的髮育是遲溝側蝕後退的一種方式,對遲溝沿線形態影響巨大,研究其成因和縯化過程對認識遲溝的側蝕和後退機製具有很大的參攷價值。基于對元謀榦熱河穀沙地村豎井群的實地攷察和測量,將豎井的髮育劃分為萌芽期、擴張期、完整期、破碎期和殘夷期5箇階段,不同髮育階段其平麵形態與剖麵形態具有顯著的差異;完整期豎井的形態最具代錶性,其長度、寬度和深度的變化範圍分彆在0.75~3.29 m、1.01~2.84 m、1.98~10.26 m,長寬比在0.3~3.1;豎井的形態與髮育過程主要受到降水和地錶徑流、構造、土體性質、地形與植被等因素的控製。這一研究有助于認識豎井的形成與縯化,也為實踐中工程地質災害防治與溝蝕鑑測提供科學指導。
수정시일충특수적잠식지모류형,시대규모토양침식배경하불용홀시적재해성배경문제。수정적발육시충구측식후퇴적일충방식,대충구연선형태영향거대,연구기성인화연화과정대인식충구적측식화후퇴궤제구유흔대적삼고개치。기우대원모간열하곡사지촌수정군적실지고찰화측량,장수정적발육화분위맹아기、확장기、완정기、파쇄기화잔이기5개계단,불동발육계단기평면형태여부면형태구유현저적차이;완정기수정적형태최구대표성,기장도、관도화심도적변화범위분별재0.75~3.29 m、1.01~2.84 m、1.98~10.26 m,장관비재0.3~3.1;수정적형태여발육과정주요수도강수화지표경류、구조、토체성질、지형여식피등인소적공제。저일연구유조우인식수정적형성여연화,야위실천중공정지질재해방치여구식감측제공과학지도。
The vertical hole is a special kind of piping landforms;it is the disastrous environmental problem that cannot be ignored under the background of large-scale soil erosion. The development of vertical hole indicates the lateral erosion of gully,so that it has a huge impact on shoulder line shape of gully. It is very important to study the evolution and formation of vertical holes for understanding the mechanics of lateral and backward erosion of gully. Based on the investigations of vertical holes at Shadi Village of Yuanmou Dry-hot Valley,they can be divided into germination period,expanding period,complete period,broken period and residual period. There are significant differences between plane shape and cross-sectional shape of vertical hole at different developmental stage. The ver-tical hole of complete period is the most representative stage,the changes of long axis,short axis and the depth of vertical holes are in the range between 0. 75~3. 29 m,1. 01~2. 84 m,1. 98~10. 26 m;the ratio of long axis and short axis is between 0 . 3~3 . 1 . The morphology and developmental process are mainly controlled by the factors of precipitation and surface runoff,structure,soil properties,terrain and vegetation etc. This paper not only contributes to the understanding of the formation and evolution of the vertical hole,but also provides scientific guidance for treatment of engineering geological hazard prevention and monitoring of gully erosion.